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Seismic stratigraphy of the Qiongdongnan deep sea channel system, northwest South China Sea

文献类型：期刊论文

作者Yuan Shengqiang1,2; Lue Fuliang3; Wu Shiguo1,4; Yao Genshun1,2,3; Ma Yubo1,2; Fu Yanhui4
刊名CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
出版日期2009-06-01
卷号27期号:2页码:250-259
ISSN号0254-4059
关键词Qiongdongnan Deep Sea Channel South China Sea Sedimentary System Sea Level Change
DOI10.1007/s00343-009-9177-0
文献子类Article
英文摘要Based on more than 4000 km 2D seismic data and seismic stratigraphic analysis, we discussed the extent and formation mechanism of the Qiongdongnan deep sea channel. The Qiongdongnan deep sea channel is a large incised channel which extends from the east boundary of the Yinggehai Basin, through the whole Qiongdongnan and the Xisha trough, and terminates in the western part of the northwest subbasin of South China Sea. It is more than 570 km long and 4-8 km wide. The chaotic (or continuous) middle (or high) amplitude, middle (or high) continuity seismic facies of the channel reflect the different lithological distribution of the channel. The channel formed as a complex result of global sea level drop during early Pliocene, large scale of sediment supply to the Yinggehai Basin, inversion event of the Red River strike-slip fault, and tilted direction of the Qiongdongnan Basin. The large scale of sediment supply from Red River caused the shelf break of the Yinggehai Basin to move torwards the S and SE direction and developed large scale of prograding wedge from the Miocene, and the inversion of the Red River strike-slip fault induced the sediment slump which formed the Qiongdongnan deep sea channel.; Based on more than 4000 km 2D seismic data and seismic stratigraphic analysis, we discussed the extent and formation mechanism of the Qiongdongnan deep sea channel. The Qiongdongnan deep sea channel is a large incised channel which extends from the east boundary of the Yinggehai Basin, through the whole Qiongdongnan and the Xisha trough, and terminates in the western part of the northwest subbasin of South China Sea. It is more than 570 km long and 4-8 km wide. The chaotic (or continuous) middle (or high) amplitude, middle (or high) continuity seismic facies of the channel reflect the different lithological distribution of the channel. The channel formed as a complex result of global sea level drop during early Pliocene, large scale of sediment supply to the Yinggehai Basin, inversion event of the Red River strike-slip fault, and tilted direction of the Qiongdongnan Basin. The large scale of sediment supply from Red River caused the shelf break of the Yinggehai Basin to move torwards the S and SE direction and developed large scale of prograding wedge from the Miocene, and the inversion of the Red River strike-slip fault induced the sediment slump which formed the Qiongdongnan deep sea channel.
学科主题Limnology ; Oceanography
语种英语
WOS记录号WOS:000267970300008
公开日期2010-12-22
源URL[http://ir.qdio.ac.cn/handle/337002/3727]  
专题海洋研究所_海洋地质与环境重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
3.PetroChina Hangzhou Inst Geol, Hangzhou 310023, Zhejiang, Peoples R China
4.China Univ Petr, Qingdao 266555, Peoples R China
推荐引用方式
GB/T 7714		 Yuan Shengqiang,Lue Fuliang,Wu Shiguo,et al. Seismic stratigraphy of the Qiongdongnan deep sea channel system, northwest South China Sea[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2009,27(2):250-259.
APA Yuan Shengqiang,Lue Fuliang,Wu Shiguo,Yao Genshun,Ma Yubo,&Fu Yanhui.(2009).Seismic stratigraphy of the Qiongdongnan deep sea channel system, northwest South China Sea.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,27(2),250-259.
MLA Yuan Shengqiang,et al."Seismic stratigraphy of the Qiongdongnan deep sea channel system, northwest South China Sea".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 27.2(2009):250-259.

入库方式： OAI收割

来源：海洋研究所

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